Show simple item record

dc.contributor.authorSomayajulu, B.L.K.
dc.contributor.authorBhushan, R.
dc.contributor.authorNarvekar, P.V.
dc.date.accessioned2009-01-10T10:01:36Z
dc.date.available2009-01-10T10:01:36Z
dc.date.issued1999
dc.identifier.citationGeophysical Research Letters, Vol.26; 2869-2872p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/1729
dc.description.abstractIndian Ocean Deep waters (IDW) show an increase in salinity and sigma CO sub(2) between 64 degrees S and 16 plus or minus 4 degrees N by 0.106-0.110 ppt and 82-104 mu M kg sup(-1) respectively with a corresponding decrease in delta sup(14)C by 42 ppt, as revealed by the GEOSECS data (1977-78). The delta sup(14)C-sigma CO sub(2)-salinity relationships show better correlation in the western sector. High biological productivity induced changes and corrosive deepwaters could account for sigma CO sub(2) increase in the northern regions. Reoccupation of GEOSECS stations during 1985-95 do not show distinctly discemible short-term temporal changes in delta sup(14)C, sigma CO sub(2) and salinity
dc.language.isoen
dc.publisherAmerican Geophysical Union
dc.rightsCopyright [1999]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectsalinity
dc.subjectcarbon dioxide
dc.subjectcarbon isotopes
dc.subjectocean circulation
dc.subjectair-water exchanges
dc.subjecttemporal variations
dc.subjectspatial variations
dc.subjectdeep water
dc.subjecttemperature
dc.titleDelta sup(14)C, sigma CO sub(2) salinity of the western Indian Ocean deep waters: Spatial and temporal variations
dc.typeJournal Article


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record